Numerical Model of the Cloud Particle Isotope Composition Formation

摘要

A non-stationary numerical model for isotope composition formation of cloud particles is developed. The improved model consists of three blocks: hydrothermodynamic, microphysical, and isotope. The latter block contains equations for calculation of isotope content in water vapor and in the cloud particles. The results of the study show that the developed approach can be applied to widen resources for interpretation of surface measurements of hail.